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At present, SSC fluxes in rivers are typically estimated by multiplying the river discharge with theaverage suspended sediment concentration (SSC). The latter is typically obtained from optical turbiditymeasurements in one single point of the river c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5418b29235e79c2249f7a7ca90b2ea7
https://doi.org/10.5194/egusphere-egu23-14356
https://doi.org/10.5194/egusphere-egu23-14356
Publikováno v:
Geomechanics and Tunnelling. 11:537-543